Coastal groundwater (CGW) is a critical water resource for many communities and can be a
key part of coastal ecosystems. Owing to its location, CGW faces both terrestrial and marine …

This paper discusses the potential response of fluvial processes and landforms to the
projected permafrost degradation and related hydrological change. Fluvial system structure …

In cold regions where soils freeze and thaw annually, the ground surface deforms due to the
density difference between groundwater and ground ice. Here we mapped thaw subsidence …

Lateral CH4 inputs to Arctic lakes through groundwater discharge could be substantial and
constitute an important pathway that links CH4 production in thawing permafrost to …

The seasonal dynamic of the suprapermafrost groundwater significantly affects the runoff
generation and confluence in permafrost basins and is a leading issue that must urgently be …

The source region of the Yangtze River (SRYR, 1.4× 105 km2 above Zhimenda station) on
the Tibetan Plateau (TP) has 78% permafrost coverage. The streamflow depth increased at …

The impacts of ongoing climate warming on cold‐regions hydrogeology and groundwater
resources have created a need to develop groundwater models adapted to these …

The presence of permafrost influences the flow paths of water through Arctic landscapes and
thereby has the potential to impact stream discharge and thermal regimes. Observations …

Warming in the Arctic is occurring at twice the rate of the global average, resulting in
permafrost thaw and a restructuring of the Arctic hydrologic cycle as indicated by increased …

Phosphorus (P) limitation often constrains biological processes in Arctic tundra ecosystems.
Although adsorption to soil minerals may limit P bioavailability and export from soils into …